activity
20082023
most citedOscillators and relaxation phenomena in Pleistocene climate theory

189 citations · 545 across the 17 of their papers we have counts for

collaborators

17 papers

physics.ao-ph2023

Multistability in a Coupled Ocean-Atmosphere Reduced Order Model: Non-linear Temperature Equations

Oisín Hamilton, Jonathan Demaeyer, Stéphane Vannitsem +1

Multistabilities were found in the ocean-atmosphere flow, in a reduced order ocean-atmosphere coupled model, when the non-linear temperature equations were solved numerically. In t…

physics.ao-ph2021

Sea-level and summer season orbital insolation as drivers of Arctic sea-ice

Claude Hillaire-Marcel, Anne de Vernal, Michel Crucifix

The sea-ice cover of the Arctic Ocean is an important element of the climate and ocean system in the Northern Hemisphere as it impacts albedo, atmospheric pressure regimes, CO2-exc…

stat.AP2018★ 4 cited

Quantifying Age and Model Uncertainties in Paleoclimate Data and Dynamical Climate Models with a Joint Inferential Analysis

Jake Carson, Michel Crucifix, Simon P. Preston +1

A major goal in paleoclimate science is to reconstruct historical climates using proxies for climate variables such as those observed in sediment cores, and in the process learn ab…

physics.ao-ph2016★ 7 cited

Effects of additive noise on the stability of glacial cycles

Takahito Mitsui, Michel Crucifix

It is well acknowledged that the sequence of glacial-interglacial cycles is paced by the astronomical forcing. However, how much is the sequence robust against natural fluctuations…

physics.ao-ph2015

Challenges for ice age dynamics: a dynamical systems perspective

Michel Crucifix, Guillaume Lenoir, Takahito Mitsui

This chapter is dedicated to the slow dynamics of the climate system, at time scales of one~thousand to one million years. We focus specifically on the phenomenon of ice ages that…

stat.AP2015★ 19 cited

Bayesian model selection for the glacial-interglacial cycle

Jake Carson, Michel Crucifix, Simon Preston +1

A prevailing viewpoint in palaeoclimate science is that a single palaeoclimate record contains insufficient information to discriminate between most competing explanatory models. R…